Pairwise scale space comparison of time series with application to climate research
In this paper, we study how sea surface temperature variations in the North Atlantic and the Norwegian Sea are correlated with the climate in the Northern Hemisphere in late Holocene. The analysis is performed by testing statistical hypotheses through novel scale space methodologies. In late Holocen...
Published in: | Journal of Geophysical Research: Oceans |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union (AGU)
2012
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/4569 https://doi.org/10.1029/2011JC007546 |
_version_ | 1829312035788161024 |
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author | Godtliebsen, Fred Holmström, L. Miettinen, A. Erästö, P. Divine, Dmitry V Koc, Nalan |
author_facet | Godtliebsen, Fred Holmström, L. Miettinen, A. Erästö, P. Divine, Dmitry V Koc, Nalan |
author_sort | Godtliebsen, Fred |
collection | University of Tromsø: Munin Open Research Archive |
container_issue | C3 |
container_start_page | n/a |
container_title | Journal of Geophysical Research: Oceans |
container_volume | 117 |
description | In this paper, we study how sea surface temperature variations in the North Atlantic and the Norwegian Sea are correlated with the climate in the Northern Hemisphere in late Holocene. The analysis is performed by testing statistical hypotheses through novel scale space methodologies. In late Holocene, the proposed techniques reveal that the climate development in the subpolar North Atlantic has been incoherent with the development in the Norwegian Sea and the Northern Hemisphere. A prominent discrepancy between the three analyzed series is identified for the periods associated with the Medieval Warm Period and the Little Ice Age. A divergence between the oceanic series and the global Northern Hemisphere temperature estimate detected in the twentieth century is in line with the inferred imprint of recent climate change which suggests accentuated warming, in particular over continental regions. Overall, the results obtained by scale space analysis underscore the significance of the northern North Atlantic in shaping the climate globally, mainly through changes in the strength and structure of the Atlantic meridional overturning circulation. |
format | Article in Journal/Newspaper |
genre | North Atlantic Norwegian Sea |
genre_facet | North Atlantic Norwegian Sea |
geographic | Norwegian Sea |
geographic_facet | Norwegian Sea |
id | ftunivtroemsoe:oai:munin.uit.no:10037/4569 |
institution | Open Polar |
language | English |
op_collection_id | ftunivtroemsoe |
op_container_end_page | n/a |
op_doi | https://doi.org/10.1029/2011JC007546 |
op_relation | FRIDAID 929777 doi:10.1029/2011JC007546 https://hdl.handle.net/10037/4569 |
op_rights | openAccess |
publishDate | 2012 |
publisher | American Geophysical Union (AGU) |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/4569 2025-04-13T14:23:25+00:00 Pairwise scale space comparison of time series with application to climate research Godtliebsen, Fred Holmström, L. Miettinen, A. Erästö, P. Divine, Dmitry V Koc, Nalan 2012 https://hdl.handle.net/10037/4569 https://doi.org/10.1029/2011JC007546 eng eng American Geophysical Union (AGU) FRIDAID 929777 doi:10.1029/2011JC007546 https://hdl.handle.net/10037/4569 openAccess VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 Journal article Tidsskriftartikkel Peer reviewed 2012 ftunivtroemsoe https://doi.org/10.1029/2011JC007546 2025-03-14T05:17:57Z In this paper, we study how sea surface temperature variations in the North Atlantic and the Norwegian Sea are correlated with the climate in the Northern Hemisphere in late Holocene. The analysis is performed by testing statistical hypotheses through novel scale space methodologies. In late Holocene, the proposed techniques reveal that the climate development in the subpolar North Atlantic has been incoherent with the development in the Norwegian Sea and the Northern Hemisphere. A prominent discrepancy between the three analyzed series is identified for the periods associated with the Medieval Warm Period and the Little Ice Age. A divergence between the oceanic series and the global Northern Hemisphere temperature estimate detected in the twentieth century is in line with the inferred imprint of recent climate change which suggests accentuated warming, in particular over continental regions. Overall, the results obtained by scale space analysis underscore the significance of the northern North Atlantic in shaping the climate globally, mainly through changes in the strength and structure of the Atlantic meridional overturning circulation. Article in Journal/Newspaper North Atlantic Norwegian Sea University of Tromsø: Munin Open Research Archive Norwegian Sea Journal of Geophysical Research: Oceans 117 C3 n/a n/a |
spellingShingle | VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 Godtliebsen, Fred Holmström, L. Miettinen, A. Erästö, P. Divine, Dmitry V Koc, Nalan Pairwise scale space comparison of time series with application to climate research |
title | Pairwise scale space comparison of time series with application to climate research |
title_full | Pairwise scale space comparison of time series with application to climate research |
title_fullStr | Pairwise scale space comparison of time series with application to climate research |
title_full_unstemmed | Pairwise scale space comparison of time series with application to climate research |
title_short | Pairwise scale space comparison of time series with application to climate research |
title_sort | pairwise scale space comparison of time series with application to climate research |
topic | VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 |
topic_facet | VDP::Mathematics and natural science: 400::Mathematics: 410::Statistics: 412 VDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Statistikk: 412 |
url | https://hdl.handle.net/10037/4569 https://doi.org/10.1029/2011JC007546 |